Cenozoic volcanism and lithospheric tectonic evolution in Qiangtang area, northern Qinghai-Tibet Plateau

2005 ◽  
Vol 48 (7) ◽  
pp. 1011 ◽  
Author(s):  
Xiaoguo CHI
Keyword(s):  
Tectonic Evolution ◽  
Tibet Plateau ◽  
Cenozoic Volcanism ◽  
Qinghai Tibet Plateau

Tectonic evolution of the Qinghai-Tibet Plateau

2012 ◽  
Vol 53 ◽  
pp. 3-14 ◽  
Author(s):  
Guitang Pan ◽  
Liquan Wang ◽  
Rongshe Li ◽  
Sihua Yuan ◽  
Wenhua Ji ◽  
...  
Keyword(s):  
Tectonic Evolution ◽  
Tibet Plateau ◽  
Qinghai Tibet Plateau

scholarly journals Tectonic evolution and uplift of the Qinghai-Tibet Plateau

Episodes ◽  
1995 ◽  
Vol 18 (1-2) ◽  
pp. 31-35 ◽  
Author(s):  
Xuchang Xiao ◽  
Ti ngdong Li
Keyword(s):  
Tectonic Evolution ◽  
Tibet Plateau ◽  
Qinghai Tibet Plateau

scholarly journals Present-Day Deformation of the Gyaring Co Fault Zone, Central Qinghai–Tibet Plateau, Determined Using Synthetic Aperture Radar Interferometry

2019 ◽  
Vol 11 (9) ◽  
pp. 1118
Author(s):  
Yong Zhang ◽  
Chuanjin Liu ◽  
Wenting Zhang ◽  
Fengyun Jiang
Keyword(s):  
Synthetic Aperture Radar ◽  
Fault Zone ◽  
Crustal Deformation ◽  
Tectonic Evolution ◽  
Slip Rate ◽  
Strike Slip ◽  
Synthetic Aperture ◽  
Tibet Plateau ◽  
Regional Tectonic ◽  
Qinghai Tibet Plateau

Because of the constant northward movement of the Indian plate and blockage of the Eurasian continent, the Qinghai–Tibet Plateau has been extruded by north–south compressive stresses since its formation. This has caused the plateau to escape eastward to form a large-scale east–west strike-slip fault and a north–south extensional tectonic system. The Karakorum–Jiali fault, a boundary fault between the Qiangtang and Lhasa terranes, plays an important role in the regional tectonic evolution of the Qinghai–Tibet Plateau. The Gyaring Co fault, in the middle of the Karakoram–Jiali fault zone, is a prominent tectonic component. There have been cases of strong earthquakes of magnitude 7 or greater in this fault, providing a strong earthquake occurrence background. However, current seismic activity is weak. Regional geodetic observation stations are sparsely distributed; thus, the slip rate of the Gyaring Co fault remains unknown. Based on interferometric synthetic aperture radar (InSAR) technology, we acquired current high-spatial resolution crustal deformation characteristics of the Gyaring Co fault zone. The InSAR-derived deformation features were highly consistent with Global Positioning System observational results, and the accuracy of the InSAR deformation fields was within 2 mm/y. According to InSAR results, the Gyaring Co fault controlled the regional crustal deformation pattern, and the difference in far-field deformation on both sides of the fault was 3–5 mm/y (parallel to the fault). The inversion results of the back-slip dislocation model indicated that the slip rate of the Gyaring Co fault was 3–6 mm/y, and the locking depth was ~20 km. A number of v-shaped conjugate strike-slip faults, formed along the Bangong–Nujiang suture zone in the central and southern parts of the -Tibet Plateau, played an important role in regional tectonic evolution. V-shaped conjugate shear fault systems include the Gyaring Co and Doma–Nima faults, and the future seismic risk cannot be ignored.

Sign in / Sign up

Export Citation Format

Share Document